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Corresponding author: Wendy Nelson ( wnelson@aucklandmuseum.com ) Academic editor: Dan Blanchon
© 2026 Wendy Nelson, Kate Neill, Roberta D'Archino.
This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Citation:
Nelson W, Neill K, D'Archino R (2026) Rimurimu – marine macroalgae – of Rangitāhua. Papahou: Records of the Auckland Museum 60: 25-32. https://doi.org/10.32912/papahou.60.179125
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The islands of Rangitāhua lie half way between the eastern North Island and Tonga. There are 18 islands and islets in the Rangitāhua chain extending about 300 km from Nugent Island in the north (29°13'54"S, 177°52'10"W) to L’Esperance in the south (31°21'16"S, 178°49'29"W). Thirteen of these are very small and steeply sided rocky outcrops with very few sheltered areas. The two largest islands are Rangitāhua (also known as Raoul Island) and Macauley Island. Rangitāhua is the indigenous title to Raoul Island as well as to the entire Kermadec Island region.
The islands of Rangitāhua are surrounded by very clear oceanic waters that are generally nutrient-poor (oligotrophic), although nutrient-rich water is brought to the surface by currents and tidal movements. Dense seabird communities on some of the Rangitāhua islands also contribute nutrients to the coastal waters and to the growth of the rimurimu.
Rimurimu can be found in a wide range of habitats – on rocky reefs, boulders, cobbles, shell rubble, pumice, coral, and, in some places, on coarse gravels and sand. They have been found from the intertidal zone through to the mesophotic zone (ca 30–150 m depth). Light available for photosynthesis declines with depth to the point where algae are no longer able to survive.
Some species at Rangitāhua are also found on mainland New Zealand, others are only found on these islands (endemic), while some species are also present in neighbouring areas of the subtropical and tropical Pacific.
Both intertidal and shallow subtidal zones on these rugged islands are exposed to strong wave action and oceanic swells. There are some distinctive features of the growth forms of macroalgae at Rangitāhua – adaptations to the conditions in the region.
Many species grow as crusts or cushions closely attached to substrates and protected from some of the energy of the waves. This prostrate growth habit is seen in species of green, brown and red algae (e.g., Fig.
Habitats of rimurimu found at Rangitāhua: Diminutive turfs are common and are made up of many species (A). Crustose forms are also common, particularly in coralline algae, but also other red, brown and green algae (B and C). Some species have stolons (1D). [A: E.Lis; B: M.Francis; C, D: R.D’Archino. CC BY 4.0].
In both the intertidal and subtidal zones there are dense patches of turf (Fig.
A number of species have stolons (e.g., Figs
Species of Caulerpa found at Rangitāhua: A. Caulerpa chemnitzia has grape to trumpet like ’leaves’; and stolons – and here is surrounded by finely branching turf species and coralline crusts. B. Caulerpa nummularia has disc-like ‘leaves’ with teeth around the edges; with stolons (bare stems creeping along and attaching to the rock surface). C. Caulerpa webbiana has very small, tightly packed ‘leaves’ around the stems, rimu-like. [A–C: R.D’Archino. CC BY 4.0].
A feature of Rangitāhua macroalgae is that most species are quite small – with the majority less than 5 or 10 cm in height. There are a few species that are taller and some of these, such as Asparagopsis taxiformis and Dictyota intermedia, can form dense beds. Some other species such as Delisea aweawetai and some species of Liagora can also reach more than 25 cm in height. The largest brown algae are species of Sargassum which appear to have an annual cycle of growth and are largest in spring and by autumn are small and inconspicuous.
In the coastal waters of the islands of Rangitāhua macroalgae are important primary producers, fixing sunlight energy and providing food for a range of invertebrates and fishes. The nutrient status and growth of macroalgae in the region are enhanced by nutrients contributed by seabirds nesting on the islands.
Although macroalgae at Rangitāhua are much less conspicuous than kelps in colder waters, they play a key role in providing three-dimensional habitat space for a range of fish and invertebrate species. They provide physical shelter and camouflage as well as surfaces for other species to settle on – ranging from bacteria to other algae and invertebrates.
Rimurimu, particularly species of coralline algae, can play key roles in life histories of other species.
Some invertebrates such as corals, settle onto coralline crusts changing from larval stages and developing into their adult forms, with their metamorphosis triggered by chemicals the coralline crusts release. Other species settle preferentially onto branched corallines – getting protection from grazers.
The green seaweeds of Rangitāhua are visually dominated by two genera (Caulerpa and Codium).
There are three species of Caulerpa at Rangitāhua (Fig.
Caulerpa chemnitzia (previously known as C. racemosa in this region) has trumpet shaped ‘leaves’ (Fig.
There are a variety of other green algae found at Rangitāhua including bushy Bryopsis, bladed species of Ulva and Ryuguphycus, and very fine, filamentous algae such as Cladophora (Fig.
Other groups of green rimurimu found at Rangitāhua: Cladophora and Lychaete are made up of fine filaments, and this example is growing on a limpet (A). Codium form velvet cushions with folds (B). This species, Codium tohuoratai was named by Ngāti Kuri. Microdictyon forms delicate, lace-like sheets (C). Palmophyllum umbracola grows as a vivid green, firm jelly-like crust (D). [A: R.D’Archino; B: M.Francis; C: E.Lis; D: B.Masters. CC BY 4.0].
The brown rimurimu of Rangitāhua are dominated by members of the order Dictyotales (Fig.
Members of the brown order Dictyotales are common at Rangitāhua. Dictyota intermedia is the largest and grows as divided strap-like blades (A). This smaller species of Dictyota is partially iridescent (B). Padina is partially calcified and found in the intertidal zone (C). There are several undescribed species of Distromium present, and they grow as golden to brown fans (D). [A: P.Caiger; B: B.Masters; C, D: R.D’Archino. CC BY 4.0].
The largest brown algae in the coastal zone belong to the genus Sargassum (Fig.
Other types of brown rimurimu found at Rangitāhua: Sargassum is the largest brown alga in the coastal zone, growing here attached to a rock among sand (A). Colpomenia forms sac-like bladders (B). Brown crusts can be found in the intertidal zone as well as subtidally growing on rock and on the shells of molluscs (C). [A: M.Francis; B: B.Masters; C: R.D’Archino. CC BY 4.0].
The kelp that grows in northern New Zealand – Ecklonia radiata – has only been found in deep colder waters of the Rangitāhua region (at 70 m depth).
Other brown algae include sacs such as Colpomenia (Fig.
There are more species of red rimurimu than the greens and browns together. Just like the greens and browns, most of the red rimurimu are small, with most less than 5 cm in height.
Asparagopsis taxiformis (Fig.
Larger red rimurimu found at Rangitāhua: Asparagopsis taxiformis (A) is often abundant and uses stolons to both hold on and spread. Delisea aweawetai (B). [A: P.Caiger; B: R.D’Archino. CC BY 4.0].
Delisea aweawetai found from the shallow subtidal to depths of ca. 30 m, is the largest species of red algae found at Rangitāhua, reaching a height of 25 cm or more, and common in the coastal reef areas. Delisea (Fig.
Martensia (Fig.
Other types of red rimurimu found at Rangitāhua: Martensia (A) forms a lace-like network around the edges of its blades. Plocamium is flattened, and its branches alternate (B). Wrangelia is very finely branched, giving it a fluffy appearance (C). [A: B.Masters; B, C: R.D’Archino. CC BY 4.0].
The coralline algae (Fig.
Coralline algae are a dominant component of the red rimurimu found at Rangitāhua. These calcified algae are very diverse and occur as crusts or turfs. Crusts that may be knobbly, lumpy or flat (A–C). Several species of Jania can be found, and form dense turfs, often dichotomously branched (D). [A: E.Lis; B: B.Masters; C, D: R.D’Archino. CC BY 4.0].
The crustose corallines vary a great deal in appearance in colour – from pale pink through to bright purple/pink – as well as texture – from smooth patches to convoluted lumpy crusts, to delicate layers and disc like growths (Fig.
There are many species belonging to a group of red algae called the Nemaliales (Fig.
Red algae in the order Nemaliales are conspicuous at Rangitāhua and vary in appearance and texture: A dichotomously branched, partially calcified species (A). A very soft and mucilaginous species (B). A flattened, dichotomously branched species (C). A species with a ‘woolly’ appearance (D). [A: P.Caiger; B–D: R.D’Archino. CC BY 4.0].
Global climate change and biodiversity loss are recognised as two of the most important challenges and risks facing the world. Climate and biodiversity are strongly linked with each other, and with the future and well-being of human communities. Rangitāhua is not immune from the global stressors linked to climate change, and rimurimu are affected by a range of climate change impacts – increased temperatures in the sea, altered patterns of rainfall, sea-level rise, increased frequency and intensity of weather events, and oxygen depletion and ocean acidification. Different species vary greatly in their responses and tolerances to these changing environmental conditions. The calcified species of rimurimu are particularly vulnerable to the impacts of ocean acidification: ocean acidification reduces coralline algal habitat complexity and is projected to adversely affect ecosystem services.
Changing conditions also influence the other marine life at Rangitāhua potentially resulting changes in the ranges and abundance of predators and herbivores which in turn are likely to influence the rimurimu of the region.
The oceanic volcanic islands of Rangitāhua occupy a unique position alongside the adjacent trench, and as such can serve as a sentinel and a bellwether of change, offering the potential to guide understanding of future trends and pathways.
This research and research collaboration acknowledges Ngāti Kuri as mana whenua and mana moana of Rangitāhua. Te Mana o Rangitāhua is an iwi-led Research Programme, funded by the Ministry for Business, Innovation and Employment (AWMMU2001) and hosted at Tāmaki Paenga Hira Auckland Museum. Collections of the species presented in this paper are housed in the Herbarium of Tāmaki Paenga Hira for reference and further research. Research is led by Ngāti Kuri through Te Ara Whanui Research Centre and undertaken with the support and guidance of Puu Kaiao – a Living Protocol for Te Mana o Rangitāhua between Ngāti Kuri and Tāmaki Paenga Hira Auckland Museum. Work on macroalgae for Te Mana o Rangitāhua has been supported by Waipapa Taumata Rau University of Auckland and New Zealand Institute for Earth Science Limited (previously NIWA). Our thanks to the photographers who provided images.